Dan Suzio Photography

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  • California poppies, Eschscholzia californica, Mount Diablo State Park, California
    07040103-california-poppy.jpg
  • California Towhee, Melozone crissalis, at Cesar Chavez Park, Berkeley, California
    18050022.jpg
  • California Towhee, Melozone crissalis, at Cesar Chavez Park, Berkeley, California
    18050021.jpg
  • California (Beechey) ground squirrel, Otospermophilus beecheyi. Hunter Mountain, in the Cottonwood Mountains of Death Valley National Park, California
    11040543.jpg
  • Students and faculty from San Jose State University, in the Greenwater Range on the eastern edge of Death Valley National Park, California
    08070195-death-valley.jpg
  • California buckeyes, Aesculus californica. Mount Diablo State Park, California
    05020007-buckeye.jpg
  • California Towhee, Melozone crissalis, perches on a railing in Benicia State Park, California
    21010287.jpg
  • California Towhee, Melozone crissalis, perches on a wire in Benicia, California
    21010285.jpg
  • California Red-sided Garter Snake, Thamnophis sirtalis infernalis, in Sonoma County, California
    19020049.jpg
  • California Towhee, Melozone crissalis, at Cesar Chavez Park, Berkeley, California
    18050018.jpg
  • California (Beechey) ground squirrel, Otospermophilus beecheyi. Hunter Mountain, in the Cottonwood Mountains of Death Valley National Park, California
    11040544.jpg
  • Sign in Wildrose Canyon, Death Valley National Park, California
    07100158-pavement-ends.jpg
  • Sign in Wildrose Canyon, Death Valley National Park, California
    07100157-pavement-ends.jpg
  • Sign on Trona-Wildrose Road, Panamint Valley, California
    07100112-watch-for-animals.jpg
  • Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070072-ryan.jpg
  • Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070076-ryan.jpg
  • Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070138-ryan.jpg
  • Ore cars at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070142-ryan-ore-car.jpg
  • Abandoned rail car at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070160-ryan.jpg
  • Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070122-ryan.jpg
  • One-room schoolhouse at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070009-ryan-school.jpg
  • One-room schoolhouse at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070030-ryan-school.jpg
  • Tadpole of California red-legged frog, Rana aurora draytonii, Contra Costa County, California. Complete life cycle available, including eggs, tadpoles, metamorphs, froglets, and adults. Red-legged frogs were once abundant throughout California, and were the inspiration for Mark Twain's classic The Celebrated Jumping Frog of Calaveras County. Now, after more than a century of habitat destruction, water pollution, suburban sprawl, and predation by non-native bullfrogs, they've been reduced to a number of scattered, unconnected populations. Federally listed as a Threatened Species.
    06100064-red-legged-frog-tadpole.jpg
  • California Towhee, Melozone crissalis, perches on a railing in Benicia State Park, California
    21010286.jpg
  • California blue-eyed grass, Sisyrinchium bellum, Mount Diablo State Park, California
    07040309.jpg
  • Card table in the American Hotel, built in 1871 at Cerro Gordo, a mining community in the Inyo Mountains near Keeler, California
    11040495.jpg
  • Inyo Mountains, near Keeler, California
    11040465.jpg
  • Seeds of California buckeye, Aesculus californica, in a streambed under the trees.  Mount Diablo State Park, California
    07260022-buckeye.jpg
  • Seeds of California buckeye, Aesculus californica, in a streambed under the trees.  Mount Diablo State Park, California
    07260021-buckeye.jpg
  • Seeds of California buckeye, Aesculus californica, in a streambed under the trees.  Mount Diablo State Park, California
    07260017-buckeye.jpg
  • Seeds of California buckeye, Aesculus californica, in a streambed under the trees.  Mount Diablo State Park, California
    07260016-buckeye.jpg
  • Seeds of California buckeye, Aesculus californica, in a streambed under the trees.  Mount Diablo State Park, California
    07260014-buckeye.jpg
  • Seeds of California buckeye, Aesculus californica, in a streambed under the trees.  Mount Diablo State Park, California
    07260012-buckeye.jpg
  • California quail, Callipepla californica, Point Reyes National Seashore, California
    07150011-quail.jpg
  • California quail, Callipepla californica, Point Reyes National Seashore, California
    07150008-quail.jpg
  • California quail, Callipepla californica, Point Reyes National Seashore, California
    07150005-quail.jpg
  • Tufa towers at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140169-mono-lake.jpg
  • Tufa towers at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140168-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140161-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140158-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140155-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140154-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140144-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140143-mono-lake.jpg
  • Pacific treefrog (Pacific chorus frog), Hyla regilla (Pseudacris regilla) on stem of California poppy, Eschscholzia californica
    07090304-treefrog.jpg
  • Pacific treefrog (Pacific chorus frog), Hyla regilla (Pseudacris regilla) on California poppy, Eschscholzia californica
    07090275-treefrog.jpg
  • Chase Pond, Mount Diablo State Park, California
    07040211-mount-diablo.jpg
  • A photographer shoots the one-room schoolhouse at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070016-ryan-school.jpg
  • Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070070-ryan.jpg
  • Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070075-ryan.jpg
  • Ore car at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070077-ryan-ore-car.jpg
  • Ore car at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070080-ryan-ore-car.jpg
  • Ore cars at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070148-ryan-ore-car.jpg
  • Abandoned mining equipment at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070149-ryan.jpg
  • Abandoned tracks at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070151-ryan.jpg
  • No Trespassing sign at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070096-ryan.jpg
  • Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070112-ryan.jpg
  • Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070114-ryan.jpg
  • Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070130-ryan.jpg
  • Students and faculty from San Jose State University, in the Greenwater Range on the eastern edge of Death Valley National Park, California
    08070189-death-valley.jpg
  • Students and faculty from San Jose State University, in the Greenwater Range on the eastern edge of Death Valley National Park, California
    08070197-death-valley.jpg
  • Stars over the Panamint Mountains, Death Valley National Park, California
    08070211-death-valley.jpg
  • One-room schoolhouse at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070036-ryan-school.jpg
  • Dormitory at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley. Visiting students from San Jose State University sleep outside on the porch overlooking Death Valley.
    08070044-ryan.jpg
  • Dormitory at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070046-ryan.jpg
  • Dormitory at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070050-ryan.jpg
  • Church at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley. Originally built at Rhyolite, Nevada, the church was dismantled and moved to Ryan when the town of Rhyolite was abandoned.
    08070061-ryan-church.jpg
  • Church at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley. Originally built at Rhyolite, Nevada, the church was dismantled and moved to Ryan when the town of Rhyolite was abandoned.
    08070062-ryan-church.jpg
  • Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070067-ryan.jpg
  • Tadpole of California red-legged frog, Rana aurora draytonii, in duckweed, Lemna sp. Contra Costa County, California. Complete life cycle available, including eggs, tadpoles, metamorphs, froglets, and adults. Red-legged frogs were once abundant throughout California, and were the inspiration for Mark Twain's classic The Celebrated Jumping Frog of Calaveras County. Now, after more than a century of habitat destruction, water pollution, suburban sprawl, and predation by non-native bullfrogs, they've been reduced to a number of scattered, unconnected populations. Federally listed as a Threatened Species.
    06100159-red-legged-frog-tadpole.jpg
  • Tadpole of California red-legged frog, Rana aurora draytonii, in duckweed, Lemna sp. Contra Costa County, California. Complete life cycle available, including eggs, tadpoles, metamorphs, froglets, and adults. Red-legged frogs were once abundant throughout California, and were the inspiration for Mark Twain's classic The Celebrated Jumping Frog of Calaveras County. Now, after more than a century of habitat destruction, water pollution, suburban sprawl, and predation by non-native bullfrogs, they've been reduced to a number of scattered, unconnected populations. Federally listed as a Threatened Species.
    06100080-red-legged-frog-tadpole.jpg
  • California slender salamander, Batrachoseps attenuatus. Mount Diablo State Park, California
    05020048-slender-salamander.jpg
  • California buckeyes, Aesculus californica. Mount Diablo State Park, California
    05020016-buckeye.jpg
  • California buckeyes, Aesculus californica. Mount Diablo State Park, California
    05020005-buckeye.jpg
  • Wood stove in the dining room of the American Hotel, built in 1871 at Cerro Gordo, a mining community in the Inyo Mountains near Keeler, California
    11040489.jpg
  • Dining room of the American Hotel, built in 1871 at Cerro Gordo, a mining community in the Inyo Mountains near Keeler, California
    11040485.jpg
  • Lobby of the American Hotel, built in 1871 at Cerro Gordo, a mining community in the Inyo Mountains near Keeler, California
    11040483.jpg
  • View of Owens Valley from Cerro Gordo Road, in the Inyo Mountains near Keeler, California
    11040479.jpg
  • Granite boulders in the Alabama Hills, near Lone Pine, California
    11040416.jpg
  • Granite boulders in the Alabama Hills, near Lone Pine, California
    11040408.jpg
  • Photographer's shadow on granite boulders in the Alabama Hills, near Lone Pine, California
    11040396.jpg
  • Algodones Dunes, Imperial County, California
    06112115.jpg
  • Pacific treefrog (Pacific chorus frog), Hyla regilla (Pseudacris regilla) on California poppy, Eschscholzia californica
    07090294-treefrog.jpg
  • Divide Meadow, Point Reyes National Seashore, California
    07150255-point-reyes.jpg
  • Bear Valley area, Point Reyes National Seashore, California
    07150229-point-reyes.jpg
  • Adopt-a-Highway sign on State Highway 1 in Marin County, California.  Friends of the White Deer is an organization opposed to the National Park Service's plans to eliminate non-native fallow and axis deer from Point Reyes National Seashore.
    07150114-deer.jpg
  • Adopt-a-Highway sign on State Highway 1 in Marin County, California.  Friends of the White Deer is an organization opposed to the National Park Service's plans to eliminate non-native fallow and axis deer from Point Reyes National Seashore.
    07150108-deer.jpg
  • California quail, Callipepla californica, Point Reyes National Seashore, California
    07150002-quail.jpg
  • Memorial bench honoring Lillie Flebbe and Dorothy Flebbe-Rives in the Big Hendy grove of coast redwoods, Sequoia sempervirens, Hendy Woods State Park, California
    08030160-redwood-memorial.jpg
  • Tufa towers at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140167-mono-lake.jpg
  • Tufa towers at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140166-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140162-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140160-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140156-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140152-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140146-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140145-mono-lake.jpg
  • Pacific treefrog (Pacific chorus frog), Hyla regilla (Pseudacris regilla) on stem of California poppy, Eschscholzia californica
    07090302-treefrog.jpg
  • Chase Pond, Mount Diablo State Park, California
    07040206-mount-diablo.jpg
  • Chase Pond, Mount Diablo State Park, California
    07040209-mount-diablo.jpg
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